Page:EB1911 - Volume 04.djvu/617

 Shiré; (3) the Nyika Plateau, which lies to the north of Angoniland; and (4) the Nyasa-Tanganyika Plateau, between the basin of the river Luangwa, the vicinity of Tanganyika and the vicinity of Lake Mweru (highest point, 7000–8000 ft.). Finally may be mentioned the tract of elevated country between Lake Bangweulu and the river Luapula, and between Lake Bangweulu and the basin of the Luangwa; and also the Lukinga (Mushinga) or Ugwara Mountains of North Western Rhodesia, which attain perhaps to altitudes of 6000 ft.

The whole of this part of Africa is practically without any stretch of desert country, being on the whole favoured with an abundant rainfall. The nearest approach to a desert is the rather dry land to the east and north-east of Lake Mweru. Here, and in parts of the lower Shiré district, the annual rainfall probably does not exceed an average of 35 in. Elsewhere, in the vicinity of the highest mountains, the rainfall may attain an average of 75 in., in parts of Mount Mlanje possibly often reaching to 100 in. in the year. The average may be put at 50 in. per annum, which is also about the average rainfall of the Shiré Highlands, that part of British Central Africa which at present attracts the greatest number of European settlers.

Geology.—The whole formation is Archean and Primary (with a few modern plutonic outbursts), and chiefly consists of granite, felspar, quartz, gneiss, schists, amphibolite and other Archean rocks, with Primary sandstones and limestones in the basin of Lake Nyasa (a great rift depression), the river Shiré, and the regions within the northern watershed of the Zambezi river. Sandstones of Karroo age occur in the basin of the Luangwa (N.E. Rhodesia). There are evidences of recent volcanic activity on the summit of the small Mlanje plateau (S.E. corner of the protectorate: here there are two extinct craters with a basaltic outflow), and at the north end of Lake Nyasa and the eastern edge of the Tanganyika plateau. Here there are many craters and much basalt, or even lava; also hot springs.

Metals and Minerals.—Gold has been found in the Shiré Highlands, in the hills along the Nyasa-Zambezi waterparting, and in the mountainous region west of Lake Nyasa; silver (galena, silver-lead) in the hills of the Nyasa-Zambezi waterparting; lead in the same district; graphite in the western basin of Lake Nyasa; copper (pyrites and pure ore) in the west Nyasa region and in the hills of North Western and North Eastern Rhodesia; iron ore almost universally; mica almost universally; coal occurs in the north and west Nyasa districts (especially in the Karroo sandstones of the Rukuru valley), and perhaps along the Zambezi-Nyasa waterparting; limestone in the Shiré basin; malachite in south-west Angoniland and North Western Rhodesia; and perhaps petroleum in places along the Nyasa-Zambezi waterparting. (See also .)

Flora.—No part of the country comes within the forest region of West Africa. The whole of it may be said to lie within the savannah or park-like division of the continent. As a general rule, the landscape is of a pleasing and attractive character, well covered with vegetation and fairly well watered. Actual forests of lofty trees, forests of a West African type, are few in number, and are chiefly limited to portions of the Nyika, Angoniland and Shiré Highlands plateaus, and to a few nooks in valleys near the south end of Tanganyika. Patches of forest of tropical luxuriance may still be seen on the slopes of Mounts Mlanje and Chiradzulu. On the upper plateaus of Mount Mlanje there are forests of a remarkable conifer (Widdringtonia whytei), a relation of the cypress, which in appearance resembles much more the cedar, and is therefore wrongly styled the “Mlanje cedar.” This tree is remarkable as being the most northern form of a group of yew-like conifers confined otherwise to South Africa (Cape Colony). Immense areas in the lower-lying plains are covered by long, coarse grass, sometimes reaching 10 ft. in height. Most of the West African forest trees are represented in British Central Africa. A full list of the known flora has been compiled by Sir W. Thiselton-Dyer and his assistants at Kew, and is given in the first and second editions of Sir H. H. Johnston’s work on British Central Africa. Amongst the principal vegetable products of the country interesting for commercial purposes may be mentioned tobacco (partly native varieties and partly introduced); coffee (wild coffee is said to grow in some of the mountainous districts, but the actual coffee cultivated by the European settlers has been introduced from abroad); rubber—derived chiefly from the various species of Landolphia, Ficus, Clitandra, Carpodinus and Conopharygia, and from other apocynaceous plants; the Strophanthus pod (furnishing a valuable drug); ground-nuts (Arachis and Voandzeia); the cotton plant; all African cultivated cereals (Sorghum, Pennisetum, maize, rice, wheat—cultivated chiefly by Europeans—and Eleusine); and six species of palms—the oil palm on the north-west (near Lake Nyasa, at the south end of Tanganyika and on the Luapula), the Borassus and Hyphaene, Phoenix (or wild date), Raphia and the coco-nut palm. The last named was introduced by Arabs and Europeans, and is found on Lake Nyasa and on the lower Shiré. Most of the European vegetables have been introduced, and thrive exceedingly well, especially the potato. The mango has also been introduced from India, and has taken to the Shiré Highlands as to a second home. Oranges, lemons and limes have been planted by Europeans and Arabs in a few districts. European fruit trees do not ordinarily flourish, though apples are grown to some extent at Blantyre. The vine hitherto has proved a failure. Pineapples give the best result among cultivated fruit, and strawberries do well in the higher districts. In the mountains the native wild brambles give blackberries of large size and excellent flavour. The vegetable product through which this protectorate first attracted trade was coffee, the export of which, however, has passed through very disheartening fluctuations. In 1905–1906, 773,919 ℔ of coffee (value £16,123) were exported; but during this twelve months the crop of cotton—quite a newly developed product, rose to 776,621 ℔, from 285,185 ℔ in 1904–1905. An equally marked increase in tobacco and ground-nuts (Arachis) has taken place. Beeswax is a rising export.

Fauna.—The fauna is on the whole very rich. It has affinities in a few respects with the West African forest region, but differs slightly from the countries to the north and south by the absence of such animals as prefer drier climates, as for instance the oryx antelopes, gazelles and the ostrich. There is a complete blank in the distribution of this last between the districts to the south of the Zambezi and those of East Africa between Victoria Nyanza and the Indian Ocean. The giraffe is found in the Luanga valley; it is also met with in the extreme north-east of the country. The ordinary African rhinoceros is still occasionally, but very rarely, seen in the Shiré Highlands, The African elephant is fairly common throughout the whole territory. Lions and leopards are very abundant; the zebra is still found in great numbers, and belongs to the Central African variety of Burchell’s zebra, which is completely striped down to the hoofs, and is intermediate in many particulars between the true zebra of the mountains and Burchell’s zebra of the plains. The principal antelopes found are the sable and the roan (Hippotragus), five species of Cobus or waterbuck (the puku, the Senga puku, the lechwe, Crawshay’s waterbuck and the common waterbuck); the pallah, tsessébe (Damaliscus), hartebeest, brindled gnu (perhaps two species), several duykers (including the large Cephalophus sylvicultrix), klipspringer, oribi, steinbok and reedbuck. Among tragelaphs are two or more bushbucks, the inyala, the water tragelaph (Limnotragus selousi), the kudu and Livingstone’s eland. The only buffalo is the common Cape species. The hyaena is the spotted kind. The hunting dog is present. There are some seven species of monkeys, including two baboons and one colobus. The hippopotamus is found in the lakes and rivers, and all these sheets of water are infested with crocodiles, apparently belonging to but one species, the common Nile crocodile.

Inhabitants.—The human race is represented by only one indigenous native type—the Negro. No trace is anywhere found of a Hamitic intermixture (unless perhaps at the north end of Lake Nyasa, where the physique of the native Awankonde recalls that of the Nilotic negro). Arabs from Zanzibar have settled in the country, but not, as far as is known, earlier than the beginning of the 19th century. As the present writer takes the general term “Negro” to include equally the Bantu, Hottentot, Bushman and Congo Pygmy, this designation will cover all the natives of British Central Africa. The Bantu races, however, exhibit in some parts signs of Hottentot or Bushman intermixture, and there are legends in some mountain districts, especially Mount Mlanje, of the former existence of unmixed Bushman tribes, while Bushman stone implements are found at the south end of Tanganyika. At the present day the population is, as a rule, of a black or chocolate-coloured Negro type, and belongs, linguistically, entirely and exclusively to the Bantu family. The languages spoken offer several very interesting forms of Bantu speech, notably in the districts between the north end of Lake Nyasa, the south end of Lake Tanganyika, and the river Luapula. In the more or less plateau country included within these geographical limits, the Bantu dialects are of an archaic type, and to the present writer it has seemed as though one of them, Kibemba or Kiwemba, came near to the original form of the Bantu mother-language, though not nearer than the interesting Subiya of southern Barotseland. Through dialects spoken on the west and north of Tanganyika, these languages of North Eastern Rhodesia and northern Nyasaland and of the Kafukwe basin are connected with the Bantu languages of Uganda. They also offer a slight resemblance to Zulu-Kaffir, and it would seem as though the Zulu-Kaffir race must have come straight down from the countries to the north-east of Tanganyika, across the Zambezi, to their present home. Curiously enough, some hundreds of years after this southward migration, intestine wars and conflicts actually determined a north-eastward return migration of Zulus. From Matabeleland, Zulu tribes crossed the Zambezi at various periods (commencing from about 1820), and gradually extended their ravages and dominion over the plateaus to the west, north and north-east of Lake Nyasa. The Zulu language is still spoken by the dominating caste in West